Avalanche Forecast

Fair

Unsettled conditions are expected for the next three days as the stormy conditions end and a ridge of high pressure begins to build. A very weak system from the coast may affect the interior regions on Sunday. Friday: A mix of sun and cloud, scattered flurries in the morning 0-2cm, treeline temperatures around -10C, ridgetop winds 20-30km/h NW easing in the afternoonSaturday: A mix of sun and cloud, mainly dry conditions, treeline temperatures around -12C, ridgetop winds light NWSunday: Cloudy with sunny breaks, scattered flurries possible 0-2cm, treeline temperatures around -15C, ridgetop winds light variable

Widespread natural and human-triggered avalanche activity up to size 3.5 was reported on Wednesday. The common theme is deep releases with around half of the reported avalanches having a slab thickness of 100-150cm. The majority of the avalanche activity is still failing on the early-Feb weak layer.From limited reports, natural activity appears to have reduced substantially on Thursday. A few naturals up to size 3 are reported but far less than on Wednesday.  One size 1 skier remote was reported and was triggered from 150m away. The peak of the natural cycle may be over but conditions for human triggering are prime and consequences remain high.

The never ending storm cycle has produced 120 - 180 cm of total snowfall across the region which is settling into a cohesive slab that averages 1m in thickness. This slab sits on a nasty persistent weak layer surface hoar/facet/crust combo that was formed during the month of cold clear weather. Field observers continue to report easily triggered sudden planar failures on this interface in snowpack tests. Large settlements and whumpfs have been reported at all elevations, even in previously skied terrain. Large natural avalanches have been widespread and destructive. We expect touchy conditions to remain in place longer than we're normally accustomed to. Recent strong winds out of the SW through NW have created wind slabs on leeward features in wind exposed areas at treeline and in the alpine. In many areas, thick wind slabs may overlie the persistent weak layer creating the conditions for very large, destructive avalanches.For the most part, the mid and lower snowpack are strong and well consolidated.